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In meteorology, convective available potential energy (commonly abbreviated as CAPE) is a measure of the capacity of the atmosphere to support the vertical movement of air that can lead to cloud formation and storms. As air rises in an atmosphere, it expands and cools. CAPE exists when a given mass of air (called an air parcel) can ascend and remain…
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cape air parcel temperature atmosphere convective values buoyancy within environment kg surrounding environments potential atmospheric given also thunderstorms may weather
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| within tropical cyclones.The numerical methodology underlying CAPE can also be performed for portions of the atmosphere where an air parcel would be denser | instance of | This calculation is better suited for humid tropical environments | 0.80 | text |
| cooler than its surroundings | instance of | This calculation is better suited for humid tropical environments | 0.80 | text |
| capping inversions can prevent air from tapping into CAPE entirely | instance of | the presence of high CAPE alone does not guarantee their development as atmospheric layers with high convective stability | 0.80 | text |
| Convective available potential energy | has application | On | 0.60 | section |
| Convective available potential energy | has application | CAPE | 0.60 | section |
| Convective available potential energy | has application | This | 0.60 | section |
| Convective available potential energy | has application | Parcel | 0.60 | section |
| Convective available potential energy | has application | In | 0.60 | section |
| Convective available potential energy | has application | Air Weather Service | 0.60 | section |
| Convective available potential energy | has application | United States Air Force | 0.60 | section |
| Convective available potential energy | has application | The | 0.60 | section |
| Convective available potential energy | has application | Other | 0.60 | section |
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